Lecture 17 RRDE

Embed Size (px)

Citation preview

  • 8/15/2019 Lecture 17 RRDE

    1/7

     

    Lecture 17.1 Hydrodynamic Methods

    Rotated Disk Electrode Voltammetry RDEV

    u l a t o r

     C o n d u c

     t o r

     e l e c t r o d

     e

      f  π  ω     2=

    ω in s-1, so f in rps  revolutions

      per second

    r 1

    “dead” or

    diffusion laye

    Laminar flow occurs up to a point, at too i! ω, we findtat tur"ulent flow occurs# $is is wen te value

    e%ceeds te Reynold&

    num"er for tat particular fluid wit a !iven kinematic

    viscosity, ν, in cm' s-1#

    2

    1

    v

    r ω  

    3

    11

    −−

    →→

    =cm g d 

     scm g nv

    (  R e ) ' % 1

     * +

    o, ω sould "e ( ' 1*+  ν.r ', "ut oter limitations actuallyean ω / 1*** s-1 or f 1*,*** rpm#

    n te low ω side, must rotate fast enou! to esta"lis constant,omo!eneous supply of material to electrode surface# ω  1* s-1

    *)??20(*2001.0~

    3

    2

    12

    C at viswhat C at  scmisv

    CN CH 

    O H 

    °°

    23oise4

    Look in $a"le 5#'#1

  • 8/15/2019 Lecture 17 RRDE

    2/7

     

    Lecture 17.2 Hydrodynamic Methods

    6f one applies a potential wic is tat needed to o"tain

    mass-transport limited conditions, ten wat is i 7

    consider8

      - ydrodynamics

      - diffusion

    9y7 

      *  x  

    δ 

    ∗o

     0  :  n  e

      R

       o n l y  0 

     p r e s e n

     t

    Recall tat δ  is ;21.ω4#

    o,

    δ 

    oooo

    t oo

     DmC mnFAi

     x

    C nFADi

    ==

    ↓≈

           ∂∂=

    ∗ ;

    ),(

    ow solve7 =s we did "efore e%cept incorporate ydrodynamics

    =lso8

      $wo Cases81# Reversi"le use

    θ e%pression 2>ernst4'# ?efore reac @$ limit

      and - irrev#

      - Auasi-rev# E$ r%ns#

    )(),0(

    ),(

    )0,(

     E  F t C 

    C t C 

    C  xC 

    o

    oo

    oo

    =

    =∞

    =∗

    Real

    profile

     @ u s t  s c a n

      E  s l o w

     l y, 

     ν  /  1 *

     *  m  V  s -

     1

  • 8/15/2019 Lecture 17 RRDE

    3/7

     

    Lecture 17.3 Hydrodynamic Methods no iDL effects#

    Case 18 Levic EAuation 

    Bnow8

    Bnow8  Levic Layer ;6.1

    62.0

    2/1

    6/13/1

    2/16/13/2

    lim

    ω 

    ν δ 

    ω ν 

     D

    C nFADi oo

    =

    =   ∗−

    f reaction is DC, ten ilim vs# ω1.' is linear wit ero intercept#

    =lso if E$ reversi"le8

    Levic plot

    i

    ii

    n D

     D

    n E  E 

    cl 

    o

     Ro  −

    +   

      

     +=   ′   ,

    3/2

    log059.0

    log059.0

    > o 

     d e p e n d e n

     c e

     o f  w a v e  s 

     a p e 

     o n  ω E

    en plot of E app

     vs# will "e strai!t wit slope V ni

    iil    059.0log   =−

    Case '=8 $otally irreversi"leF 0 only

    ?ut,k 

    f  is ;2E 

    4 , so we denote tisk 

    f 2E 

    4#

    9e call tis current iB and it is8

    $is is te Binetic current#

    o, at i! enou! - , we sould !et k  77 >0#

    [ ]∗∗ −=   R  bo  C k C k nFAi

    ( )   ∗=   o !    C  E nFAk i

    ( )

      −−°=′

     RT 

     E  E  F nk k 

    o

    aα e"# 

    E 1.'

    Gero

  • 8/15/2019 Lecture 17 RRDE

    4/7

     

    Lecture 17.$ Hydrodynamic Methods

      E1

      E'  EH

      EI2on i li

    9e ave no E$ effects at -η,6rrev# Rev# for i, so we merely !et ilim 

    ic

    : -

    ia

    o, if we could vary E  and measure iB, we

    could !et 77°k 

    E  vs Ref 

    E$ effects

    ?-V . >o @$

    @$ effects

    Jes

  • 8/15/2019 Lecture 17 RRDE

    5/7

     

    Lecture 17.5 Hydrodynamic Methods

    [ ] RT  F nk  E k  RT 

     F n

    k  E  E k 

     E k C  A F n

     E C  E nFAk 

    a

    o

     f  

    a

    oo

     f  

    i f  o

    app

    o f  

    /e"#)( %&'?

     ilo#elo,

    .l*o i*terce#tget+*)(or-.l*lot

    .+tet.,,,

    *o %e.+t)(

    1 i*terce#tgeteo,

    η α 

    α 

    η 

    −=

    −=

       

      

     

    Case '?8 uasi Reversi"le for 0 and R

    >ow we ave "ot k f  and k b a function of n# $us, teBouteckK Levic plots do not ave same slope for various

    3otentials 2η4#

    3ro"lems @inimie errors "y usin! small potential ran!e

    near te foot of te wave were i  is not can!in! so drastically

    ( )[ ] RT  E  E nF k 

    i

    i

    i

    i

    o

    al cl o

    /e"#

    1

    1

    1

    ,

    1

    ,

    −−

    −°=

       

      

     ++

    −=

    α α α 

    ;nc2E4 E$

    @$7

    D o  t  i s  o n

      y o u r 

    o w n#

  • 8/15/2019 Lecture 17 RRDE

    6/7

     

    Lecture 17.6 Hydrodynamic Methods

    RRDE

    r '

    r H

    r 1

    r 1  disk radius

    r '  r 1  !ap

    r H  r '  widt of rin!≡≡

    2R4 Rin!

    2D4 Disk

    δR

    δD

    δR ) δD 

    $e collection Efficiency, N , is defined as

    6t is a ;unction of electrode !eometry "ut is independent

    of etc# if R is sta"le#

    kcem

    6f R G occurs, ten N e%ptl / N teo and N  ) ;2ω4#

    ,,,,  Roo  D DC ∗

    ω 

    i

    i N    −=

  • 8/15/2019 Lecture 17 RRDE

    7/7

     

    Lecture 17.7 Hydrodynamic Methods

    or RRDE Collection E%periments8

    1# E Rin! is eld positive enou! so as to o%idie any R#

    '# >o "ulk

    H# E Disk is scanned#

    I# i Disk is measured#

    +# i Rin! is measured#

    0,R R   =

      iD,c  0 : ne R

    E Rin!

      iD,lim

    : - E Disk vs# Re

      iR,lim

      R 0 : ne

      iR,a 

    )(

    14;293.0t+ble

    +,7or 

    .ire+ctio+t+bleii )(

    ,

    ,

    2/12/1

    ω 

    ω α ω α 

    ω 

     F  N  RRDE 

    i

    i

    i

    i D!"CA R

    iiC  D

    C  D R F ii N 

    c p

    a p

     F 

     R D

     D

     R

    ==−

    −≠−=

    Review8